Press releases

AWI hosts the King and Queen of the Netherlands

Experts from the Netherlands and the State of Bremen intensify their cooperation on coastal, marine and polar research

On the evening of 6 March 2019, His Majesty King Willem-Alexander and Her Majesty Queen Máxima of the Netherlands will visit the Alfred Wegener Institute as part of their tour of the State of Bremen. Dutch and German researchers will report to the royal couple on their collaborations regarding climate change, biodiversity and nature conservation, sign a joint declaration, and subsequently gather for a festive dinner.

A dinner at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) will round out the royal couple’s visit to the State of Bremen. “We are delighted that King Willem-Alexander and Queen Máxima of the Netherlands are interested in the polar and marine research conducted in the State of Bremen,” says AWI Director Antje Boetius. Bremen’s Mayor, Carsten Sieling, and his wife Alexia Sieling will accompany the royal couple for the duration of their visit to Bremen, which will also involve a business delegation led by the Netherlands’ Minister for Foreign Trade and Development Cooperation, Sigrid Kaag. In Bremen, key topics will be aerospace and the historical ties between the two countries. In Bremerhaven, the first stop on the agenda is the Fraunhofer Institute for Wind Energy Systems, where the focus will be on offshore wind energy, before turning to polar and marine research.

In turn, at the Alfred Wegener Institute the focus will shift to Dutch-German scientific collaboration: in the afternoon, 50 researchers from Utrecht, the isle of Texel, Groningen and Amsterdam, and from Bremen, Potsdam and Bremerhaven, will meet. “As coastal lands and important international actors in marine research, both countries face the significant challenges posed by climate change – for the research community, and for society as a whole,” says Antje Boetius. “As such, sea-level rise, the warming and acidification of the ocean, and the impacts of the change on marine organisms are major concerns,” the AWI Director adds. “Working together, we can especially contribute to understanding the role of the ocean and the polar regions for the Earth and human life.”

At a symposium, the experts will discuss changes in the Arctic and Antarctic, our coasts, the global carbon cycle, and the climate, and will plan future collaborations. The participating researchers hail from the Royal Netherlands Organisation for Scientific Research (NWO), the University of Utrecht, and the Institute for Sea Research (NIOZ), as well as the MARUM Center for Marine Environmental Sciences at the University of Bremen, and the Alfred Wegener Institute. That evening, they will sign a joint declaration on research collaboration, with the royal couple in attendance.

“During the symposium, we want to seize the opportunity to think ‘outside the box,’ says AWI bio-geologist Jelle Bijma. Dutch by birth, Bijma has organised the symposium, which he hopes will be the source of exciting discussions: “For example, we want to identify what future changes we can expect to see in the Earth system. What will climate change mean for marine ecosystems, how quickly will the sea level rise, and what parts of the climate system will be irrevocably lost if global warming continues unchecked, so that global temperatures rise by 4 to 6°C by the end of the century? And, in contrast, which functions can we preserve if we achieve the 2°C target, or even limit the rise to just 1.5 °C?” He and his colleagues will present the outcomes of the workshop to the royal couple before they all join in the festive dinner.

From 10 pm on 6 March, you can find the latest photos at: https://www.awi.de/en/about-us/service/press.html

For a detailed agenda of the royal visit, please consult the following press release from the Royal House of the Netherlands (German language): https://www.koenigshaus.nl/aktuelles/nachrichten/2019/02/11/konig-und-konigin-besuchen-bremen-%E2%80%93-programm

Contact

Science

Jelle Bijma
+49(471)4831-1831

Press Office

Folke Mehrtens
+49(0)471 4831-2007

Downloads

Im Rahmen des Projekts RESTORE vom Alfred-Wegener-Institut und Bundesamt für Naturschutz nutzen AWI-Biologen Austernkäfige, um die Lebensbedingungen der Europäischen Auster nahe eines Windparks vor Helgoland zu erforschen.
North Sea off Helgoland. (Photo: Alfred Wegener Institute / Heiner Mueller-Elsner)
Auf dem Rückweg: Die Küste Südamerikas ist in Sichtweite. 


Polarsternexpedition ANT-XXIX/6; 8. Juni - 12. August 2013; Kapstadt-Punta Arenas
Ziel der Expedition: Ein interdisziplinäres Forschungsprogramm in Atmosphäre, Meereis, Ozean und Ökosystem im antarktischen Winter, um die physikalischen und biogeochemischen Eigenschaften und Prozesse während der Wachstumsphase des Meereises besser zu verstehen. Fahrt war die erste antarktische Winterexpedition seit dem Jahr 2006. (Kurs wie im Winterexperiment 1992) 


English
There is land: On its way to Punta Arenas the research vessel Polarstern passes the coastal mountains on the Southern tip of South America. 

Polarsternexpedition ANT-XXIX/6; 8. June - 12. August 2013; Cape Town -Punta Arenas (Chile); The aim of the cruise is to carry out an interdisciplinary research programm on atmosphere, sea ice, ocean, and ecosystem during winter to obtain an understanding of physical and biogeochemical properties and processes during the sea ice growth season. It was the first Antarctic winter expedition since the year 2006.
There is land: On its way to Punta Arenas the research vessel Polarstern passes the coastal mountains on the Southern tip of South America. (Photo: Alfred Wegener Institute / Mario Hoppmann)
Sedimentschleier im Wasser vor der Küste Herschel Islands. Die Sedimente kommen entweder von kleinen Flüssen entlang der Küste oder von Küstenerosion. 

English:
Sediment clouds in the water, either caused by rivers or coastal erosion. Herschel Island, Kanada

The Alfred Wegener Institute Helmholtz Center for Polar and Marine Research (AWI) commenced research in the western Canadian Arctic with the funding of the young researcher project titled Coastal Permafrost Erosion (COPER) in 2012. The groupís focus lay on investigating the mass transfer of sediments and carbon across the whole coastal tract of , i.e. include both the emergent and submerged parts of the coast of Herschel Island, Beaufort Sea, Canada.

Herschel Island (69.6∞N, 139∞W) is located in the Beaufort Sea, at the northernmost point of the Yukon Territory, and about 70 km east of the Alaskan border. The island is a push-moraine that formed during the westward advance of of the Laurentide Ice Sheet. The coast is characterized by high cliffs and numerous retrogressive thaw slumps, indicating the presence of large massive ice bodies susceptible to permafrost degradation.  The tundra covered island is located where mean annual temperatures are well below 0∞C, and rise above freezing only between June and September. Cold temperatures affect coastal processes, as well.  Wave- and tide induced processes are limited by the presence of sea ice and landfast ice. The presence of ice, however, introduces some physical processes unique to cold environments such as ice gouging, ice rafting, ice push-up, and ice pile-up. Ice gouging refers to the grounding of ice keels; ice rafting the transport of coarse sediment offshore incorporated into the ice matrix; while ice push-up and pile-up occur at the land-sea boundary, transporting sediments on- and across shore. Coastal erosion is limited to the period of open water. Average rates of erosion are 1-2 m/yr, and may reach 10-30 m/yr.
Sediment clouds in the water, either caused by rivers or coastal erosion. Herschel Island, Canada (Photo: Alfred Wegener Institute / Jaroslav Obu)
de: Wolken von Zugvögeln sieht man im Frühjahr und Herbst über den Sylter Wattflächen
en: Clouds of migratory birds are seen over te Wadden sea near by Sylt
Clouds of migratory birds are seen over the Wadden sea near Sylt (Photo: Alfred Wegener Institute / Christian Buschbaum)
de: Wellengang in der Nordsee. Aufnahme vom Bord eines Schiffes.
en: Waves
Waves North Sea (Photo: Alfred-Wegener-Institut)
de: Ausgedehnte Betten des Fingertanges Laminaria digitata ziehen sich als dichter Gürtel von Braunalgen um die Felsküsteninsel Helgoland (Nordsee)
en: Extensive beds of brown kelp Laminaria digitata form a dense girdle around the roky island of Helgoland (North Sea)

Autor: AWI Bremerhaven
Extensive beds of brown kelp Laminaria digitata form a dense girdle around the rocky island of Helgoland (North Sea) (Photo: Alfred Wegener Institute / Inka Bartsch)
Vor der Küste Spitzbergens. Off the coast of Spitzbergen.
Off the coast of Spitsbergen. (Photo: Alfred Wegener Institute / Kristina Bär)
Wissenschaftler des Alfred-Wegener Institutes auf dem Weg zur Steilküste von Herschel Island, Kanada

English: 
Scientists from the Alfred-Wegener Institute on their way to the cliffs of Herschel Island, Canada

The Alfred Wegener Institute Helmholtz Center for Polar and Marine Research (AWI) commenced research in the western Canadian Arctic with the funding of the young researcher project titled Coastal Permafrost Erosion (COPER) in 2012. The groupís focus lay on investigating the mass transfer of sediments and carbon across the whole coastal tract of , i.e. include both the emergent and submerged parts of the coast of Herschel Island, Beaufort Sea, Canada.

Herschel Island (69.6∞N, 139∞W) is located in the Beaufort Sea, at the northernmost point of the Yukon Territory, and about 70 km east of the Alaskan border. The island is a push-moraine that formed during the westward advance of of the Laurentide Ice Sheet. The coast is characterized by high cliffs and numerous retrogressive thaw slumps, indicating the presence of large massive ice bodies susceptible to permafrost degradation.  The tundra covered island is located where mean annual temperatures are well below 0∞C, and rise above freezing only between June and September. Cold temperatures affect coastal processes, as well.  Wave- and tide induced processes are limited by the presence of sea ice and landfast ice. The presence of ice, however, introduces some physical processes unique to cold environments such as ice gouging, ice rafting, ice push-up, and ice pile-up. Ice gouging refers to the grounding of ice keels; ice rafting the transport of coarse sediment offshore incorporated into the ice matrix; while ice push-up and pile-up occur at the land-sea boundary, transporting sediments on- and across shore. Coastal erosion is limited to the period of open water. Average rates of erosion are 1-2 m/yr, and may reach 10-30 m/yr.
Scientists from the Alfred Wegener Institute on their way to the cliffs of Herschel Island, Canada. (Photo: Alfred Wegener Institute / Jaroslav Obu)
Erodierende Steilküstenregion auf der Herschel-Insel, Yukon, Kanada

English:
Eroding cliff line region on Herschel Island, Yukon, Canada

The Alfred Wegener Institute Helmholtz Center for Polar and Marine Research (AWI) commenced research in the western Canadian Arctic with the funding of the young researcher project titled Coastal Permafrost Erosion (COPER) in 2012. The groupís focus lay on investigating the mass transfer of sediments and carbon across the whole coastal tract of , i.e. include both the emergent and submerged parts of the coast of Herschel Island, Beaufort Sea, Canada.

Herschel Island (69.6∞N, 139∞W) is located in the Beaufort Sea, at the northernmost point of the Yukon Territory, and about 70 km east of the Alaskan border. The island is a push-moraine that formed during the westward advance of of the Laurentide Ice Sheet. The coast is characterized by high cliffs and numerous retrogressive thaw slumps, indicating the presence of large massive ice bodies susceptible to permafrost degradation.  The tundra covered island is located where mean annual temperatures are well below 0∞C, and rise above freezing only between June and September. Cold temperatures affect coastal processes, as well.  Wave- and tide induced processes are limited by the presence of sea ice and landfast ice. The presence of ice, however, introduces some physical processes unique to cold environments such as ice gouging, ice rafting, ice push-up, and ice pile-up. Ice gouging refers to the grounding of ice keels; ice rafting the transport of coarse sediment offshore incorporated into the ice matrix; while ice push-up and pile-up occur at the land-sea boundary, transporting sediments on- and across shore. Coastal erosion is limited to the period of open water. Average rates of erosion are 1-2 m/yr, and may reach 10-30 m/yr.
Eroding cliff line region on Herschel Island, Yukon, Canada (Photo: Alfred Wegener Institute / Jaroslav Obu)
Schneebedeckte Steilküste von Trinity Island. 

Snowy cliff line of Trinity Island.
Snowy cliff line of Trinity Island. (Photo: Alfred Wegener Institute / Thomas Ronge)